(Fig. 1) Stable carbon and oxygen isotope ratios of foraminifera of ODP Hole 113-690B ...
A remarkable oxygen and carbon isotope excursion occurred in Antarctic waters near the end of the Palaeocene (~57.33 Myr ago), indicating rapid global warming and oceanographic changes that caused one of the largest deep-sea benthic extinctions of the past 90 million years. In contrast, the oceanic...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1991
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.770081 https://doi.pangaea.de/10.1594/PANGAEA.770081 |